| Boundary
age (Ma) |
Eon | Era | Period | Epoch | Events and Life |
| 0.011 | P
h a n e r o z o i c |
C
e n o z o i c |
Quaternary | Holocene | Humans arrive, ecology changes |
| 1.8 | Pleistocene | Dramatic climate oscillations, rise & fall of sea-level cutting scarps along major rivers; ice sheets cover & uncover Ct.; | |||
| 5.0 | Tertiary | Pliocene | Marine coastal sedimentation | ||
| 23 | Miocene | erosional interval | |||
| 38 | Oligocene | erosional interval | |||
| 54 | Eocene | Semi-tropical plants in Vermont | |||
| 66 | Paleocene | erosional
interval; mammals expand
(mass extinction) |
|||
| 146 | M
e s o z o i c |
Cretaceous | Shallow sea covers coastal New England (sand now under L.I. Sound); inland regions erode with uplift; birds expand | ||
| 201 | Jurassic | Atlantic
Ocean opens, south-flowing rivers (Ct., Thames, etc.) develop; climate
becomes wetter; dinosaurs expand
(mass extinction) |
|||
| 250 | Triassic | Rifting
of Pangaea begins: Deposition of land sediments in Hartford rift basin;
SW-flowing rivers meander in semi-arid climate; primitive dinosaurs
(mass extinction) |
|||
| 286 | P
a l e o z o i c |
Permian | ALLEGHANIAN OROGENY: Alleghanian mountain building due to continental collision; Stony Creek granite and eastern pegmatites form; Pangaea completed | ||
| 325 | Pennsylvanian | Coals deposited in coastal swamps in SE New England, Alleghanian orogeny begins | |||
| 360 | Mississippian | Passive margin sedimentation; early amphibians crawl ashore | |||
| 410 | Devonian | ACADIAN OROGENY: Sediments from Acadian mountains deposited in eastern Ct; granites & western pegmatites melted by deep burial, rocks metamorphosed | |||
| 440 | Silurian | Taconic highlands eroded; submarine basin in central New England continues to be buried; early land plants | |||
| 505 | Ordovician | TACONIC OROGENY: rocks in western Ct. moved; marine muds and sands in central Ct. buried and metamorphosed | |||
| 544 | Cambrian | Carbonate deposition on passive margin; marbles in NW Ct.; earliest shelled fossils ("Cambrian explosion") | |||
| 650 | P
r o t e r o z o i c |
Neoproterozoic | 600-550: Late phase of Iapetan rifting (some basalts extruded) | ||
| 900 | 750-700: Early phase of Iapetan rifting | ||||
| Mesoproterozoic | 1100-950: GRENVILLIAN OROGENY | ||||
| oldest basement rocks in NW Ct. | |||||
| 1600 | |||||
| Paleoproterozoic
|
oxygen increases | ||||
| 2500 | |||||
|
A
|
|||||
| 3800 | Atmosphere develops | ||||
|
H
|
|||||
| Earliest signs of life (bacteria) | |||||
| 4600 | Formation of the Earth and cooling of the crust | ||||